in winter The Chikuma River rises in the northeastern foothills of
Mount Kobushi in the Japanese Alps on the border of
Saitama,
Yamanashi and Nagano Prefectures, partially in the
Chichibu Tama Kai National Park It joins with the Yochi River and flows roughly north to join the () then turns northwest into an
intermontane basin at
Nagano City where it is joined by the Sai River from
Matsumoto and the Hoshina River (). The Chikuma then changes direction and flows northeast from Nagano into Niigata Prefecture where it changes its name to the Shinano River. The Shinano continues northeast to a
confluence with Uono River between
Ojiya and
Uonuma (). After its confluence with Uono River, the Shinano is crossed by
Koshiji Bridge and the
Shinetsu train line before emerging onto
Echigo Plains of the Niigata Prefecture at
Sanjō. After entering the Echigo Plains the river becomes
deltaic and swampy due to its very small gradient (an average of 1 in 4000).
Ōkōzu Diversion Channel Due to seasonal high rainfall in the Shinano's watershed the fertile farmlands on the Niigata plain were subjected to flooding every three to four years which destroyed crops, particularly rice, and villages. Attempts from local residents to secure funding to build a diversion channel began in the mid-early eighteenth century, during the
Kyōhō era. The construction of the diversion channel has resulted in marsh fields drying on the Niigata plain which allows for greater production. Likewise, drier land has also allowed for the construction of infrastructure such as expressways and the
Shinkansen express-train network, to support a greater population in the area.
Sekiya Diversion Channel ; Shinano River; Sekiya diversion channel Flooding in the Niigata area continued following the construction of the Ōkōzu Channel. As a result, another channel, which was originally planned in the
Edo period (1700s–1800s), was built on the western outskirts of Niigata City to further mitigate the risk of flooding and to help prevent
saltwater intrusion into the Shinano estuary. The Sekiya Diversion Channel was originally to be funded by the Niigata Prefecture; however the
1964 Niigata earthquake resulted in the funds no longer being available so it was adopted as a national project. Construction of the Sekiya Diversion Channel commenced in 1968 and concluded in 1973 with a channel long and wide. The channel provides another alternate path for sediment to be directed straight out to sea and away from the Niigata port. The channel is crossed by the
Echigo Line and the
National Route 402 (excavated materials from the channel were used in the construction of Route 402).
Major dams There are a number of major dams in the Shinano River system, but not on the main river itself, rather its tributaries are extensively dammed and used for electricity generation as well as water for irrigation. The major dams in the system are listed below: It is also the second tallest dam in Japan, after the
Kurobe Dam. • The Nanakura Dam, which is part of the Takase Dam system, holds . • The
Nagawado Dam is on the
Azusa River, another tributary of the Sai, holds and is followed downstream by a number of smaller dams including the
Midono Dam and
Inekoki Dam. • The
Sagurigawa Dam sits on the Sankuni River which is a tributary of the Uono River. It holds and is used for a range of purposes including storage for power generation, flood control and water for irrigation. ==Watershed==